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Solution Etching of Detrital Staurolite

Published online by Cambridge University Press:  01 May 2009

Geoffrey Bond
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Extract

Attention has recently been directed, particularly by the writings of Boswell (1942) and Smithson (1941, 1942), to the instability of detrital minerals. In nearly all cases where etching of mineral grains has been described the rocks have been deposited under water, as members of a continuously sedimentary series.

Information

Type
Articles
Information
Geological Magazine , Volume 80 , Issue 4 , August 1943 , pp. 155 - 156
Copyright
Copyright © Cambridge University Press 1943

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References

List of Works to Which Reference is Made

Boswell, P. G. H., 1942. Anniversary Address. Quart. Journ. Geol. Soc., xcvii, Ivi.Google Scholar
Dana, . Textbook of Mineralogy, 4th ed., p. 638.Google Scholar
Frost, A., 1927. Notes on an Occurrence of Quartzite at Gwaai S.R. S.A. Journal Sci., xxiv, 177–181.Google Scholar
Smithson, F., 1941. Alteration of Detrital Minerals in the Mesozoic rocks of Yorkshire. Geol Mag., Ixxviii, 97–112.CrossRefGoogle Scholar
Smithson, F., 1942. The Middle Jurassic Rocks of Yorkshire: A Petrological and Palaeographical Study. Quart. Journ. Geol. Soc., xcviii, 1942, 27.CrossRefGoogle Scholar